"climatic equilibrium" is correct and can be used in written English.
It is used to refer to a balance in the Earth's climate system brought about by the interaction of the atmosphere, oceans, soils, and biota. For example, you could say: "The Earth's climatic equilibrium has been thrown off balance due to human activities, leading to global warming."
The observed range of a species reflects multiple determinants, including climatic tolerances, biotic interactions, equilibrium with climate and dispersal limitation.
Measured by dilatometry after reaching the equilibrium in climatic chambers Fig. 3 Kinetics of hydric swelling of the repair mortar and, in the inset, of the Ostermundigen Blue sandstone.
Global climatic changes alter the equilibrium of many ecosystems and the distribution of species they support [1], [2].
However, SDM predictions may be prone to errors if species are not at equilibrium with climatic conditions in the current range and if training samples are not representative.
First, a species is assumed to be at equilibrium with climatic conditions in the current range; i.e., a species is present in almost all regions of the training area where climatic conditions are suitable.
A portion of the SOC in subsurface horizons of modern soils was likely inherited from the Brady Soil, which probably formed in a climate different than the present, suggesting that SOC storage is probably not in equilibrium with modern climatic conditions.
One reason stems from a mind-set of experts who only know about equilibrium environments, in which climatic conditions are predictable and factors other than rainfall have measurable effects on production.
When the rate of temperature change exceeds the rate of dispersal in a geographic domain, or when dispersal rates are characterized by pronounced interspecific variation, species will be in non-equilibrium with respect to the climatic gradients that exert either direct or indirect influences on their realized niches.
The exhibition comes out of an ecologically conscious standpoint, with works that hope to "reflect a fragile equipoise between creation and destruction, evoking the dynamic equilibrium underlying the biological, environmental, and climatic systems that facilitate life," according to the press release.
There also is a place for cycles of erosion of several kinds and for dynamic equilibrium, either as an end phase of enduring climatic morphogenesis and/or as an end phase of relief and elevation reduction by denudation following orogenesis.
